Abstract
Ten acid sources, including granular and powdered forms of elemental S, iron sulfate slag, ferrous sulfate, and ammonium sulfate were added in equivalent amounts to two Histosols and three Alfisols typical of soils from the Everglades, and the soils were incubated for over 6 mo. At 2240 kg S ha−1, the powdered form of S was more effective in lowering soil pH than the granular sources of S. Little difference was found between the granular S products. Ferrous sulfate and ammonium sulfate lowered soil pH more than the elemental S products.
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